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Journal of Theoretics

Abstract: "Time Equivalence of the Tropical Year and the Sidereal Year"

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Author: Uwe Homann

Published in the Scientific Peer-Reviewed Journal of Theoretics, Vol.3 No.3 June/July 2001

The defined length of the mean solar day is based solely on the precise length of the tropical year. It is not derived from a roughly twenty minutes longer sidereal year. A wobbling Earth's axis is a physical motion that only creates an illusion of time. Think about it: A hypothetical non-rotating and non-orbiting Earth, wobbling on its polar axis does not produce a physical time period equal to the defined measure of the tropical year, no matter how long it would take for the axis to describe a complete circle in space

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